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oxygen
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Chordata
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Indian Ocean
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Integrated Ocean Drilling Program
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Expeditions 320/321
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Expedition 321
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IODP Site U1338 (1)
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Invertebrata
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Mollusca
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Protista
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Rotaliina
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Cassidulinacea
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Nodosariacea (1)
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Textulariina
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isotopes
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Mediterranean Sea (1)
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metamorphic rocks
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Ocean Drilling Program
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Leg 166
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ODP Site 1006 (1)
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oxygen
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Pacific Ocean
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sediments
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spolia
Geology and Cultural Heritage: characterization and provenance of local stones and spolia used in the Romanesque façade of Santa Maria della Piazza church (Ancona, Central Italy)
From spolia to recycling: the reuse of traditional construction materials in built heritage and its role in sustainability today: a review
Abstract The reuse of traditional construction materials attests to their high value over the long term. In fact, the practice has always demonstrated the inherent value of traditional raw materials and their products in confronting the issues of sustainability, in the broader sense of preserving resources – material and immaterial – for future generations. Throughout the history of building, the symbolic value of spolia (i.e. the use of ancient architectural elements in new construction) has gone hand-in-hand with the practice of recycling, demonstrating, at various levels, an intrinsic awareness of reuse as a tool for minimizing waste of materials and energy. Today, sustainability is rarely considered from a long-term perspective, and when it is, the approach tends to be from a broad theoretical standpoint. In the past, however, it was a common and necessary aspect of construction management, when the waste of materials was a forbidden luxury. This paper presents a review of the reuse of geomaterials, mainly stone, throughout the Italian history of construction, indicating major examples selected for their value as memorable references, describing common practices from antiquity to modern times, and concluding with a description of the actual state of the art of the practice, based on very recent and outstanding cases.
The central photo shows a view of the Tolbiacum excavation in April 2001 fr...
A new species of microforaminifera ( Gavelinopsis caledonia ) from the continental shelf, west of Scotland
A NEW SPECIES REPRESENTING THE OLDEST APHID (HEMIPTERA, APHIDOMORPHA) FROM THE MIDDLE TRIASSIC OF CHINA
ON THE ROTALIINE NATURE OF GAVELINOPSIS
The Use of Engineering Seismological Models to Interpret Archaeoseismological Findings in Tolbiacum, Germany: A Case Study
ALPHA AND BETA DIVERSITIES OF LATE QUATERNARY BATHYAL BENTHONIC FORAMINIFERAL COMMUNITIES IN THE NE CARIBBEAN SEA
Rhinocerotidae from the early Miocene of the Negev (Israel) and implications for the dispersal of early Neogene rhinoceroses
The first record of the Permian Glossopteris flora from Sri Lanka: implications for hydrocarbon source rocks in the Mannar Basin
Late Quaternary benthonic foraminifera in a bathyal core from the Leeward Islands, Lesser Antilles, NE Caribbean Sea
SYSTEMATIC TAXONOMY OF EARLY–MIDDLE MIOCENE PLANKTONIC FORAMINIFERA FROM THE EQUATORIAL PACIFIC OCEAN: INTEGRATED OCEAN DRILLING PROGRAM, SITE U1338
MOLECULAR PHYLOGENY OF COMMON CIBICIDIDS AND RELATED ROTALIIDA (FORAMINIFERA) BASED ON SMALL SUBUNIT rDNA SEQUENCES
Late Pliocene to Early Pleistocene Planktonic Foraminifera from Northern Indian Ocean (Andaman and Nicobar Islands): Interpretation on Cooling Event and Ocean Upwelling
ECOSTRATIGAPHIC REGIME SHIFT DURING LATE QUATERNARY MARINE ISOTOPE STAGES 8–9 IN SANTAREN CHANNEL, WESTERN TROPICAL ATLANTIC OCEAN: BENTHONIC FORAMINIFERAL EVIDENCE FROM ODP HOLE 1006A
The main morphological trends in the development of the foraminiferal aperture and their taxonomic significance
Distribution patterns of Recent pteropods in surface sediments of the western continental shelf of India
FORAMINIFERAL ASSEMBLAGE FORMATION IN DEPOSITIONAL SINKS ON THE CONTINENTAL SHELF WEST OF SCOTLAND
History and development of methods in Recent benthic foraminiferal studies
Abstract Sometime in the course of the second millennium BC , an earthquake appears to have triggered a massive eruption of the Santorini volcano. The immediate consequences of the earthquake closely followed by the eruption for Cretan society during the Late Minoan I period are rather difficult to characterize, although physical evidence in the form of Theran ash has shown up at an increasing number of sites. Certain features of the archaeological record, taken in isolation, have hardly been noticed in the past. The long-term effects of the eruption, however, have recently become more comprehensible thanks to a reconsideration of old and new archaeological evidence. The combined picture gives the impression of a period of societal stress following these events. Changes in architecture, storage and food production, artisan output, the distribution of prestige items, administrative patterns and ritual manifestations can be pinpointed archaeologically. These may and should be interpreted as disturbances in the political, economic, cult and security-related domains. It is argued that the inability of the Minoan palatial centres to adapt to changing circumstances caused by a double disaster, an earthquake followed by the eruption of Santorini, led to an increase in crisis-related situations, culminating in the widespread fire destructions which brought this palatial phase of Minoan civilization to an end and opened the way for mainland Mycenaean domination of the Aegean.